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pedrizite

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Journal Article
Published: 01 June 2015
European Journal of Mineralogy (2015) 27 (3): 417–426.
...: Ferro-pedrizite, a new amphibole-supergroup mineral was discovered in the Sutlug pegmatite occurrence situated in the Targi River Basin, Tyva Republic, Eastern Sibera, Russia. The associated minerals are quartz, albite, microcline, spodumene, cassiterite, beryl, columbite-(Mn), fergusonite-β-(Y...
FIGURES | View All (6)
Journal Article
Published: 01 April 2005
American Mineralogist (2005) 90 (4): 732–736.
... that the sample consists of a mixture of two distinct amphibole compositions, tremolite and a new amphibole end-member, fluoro-sodic-pedrizite, ideally A Na B Li 2 C (Mg 2 Al 2 Li) T Si 8 O 22 X F 2 (IMA-CNMMN 2004-002). Fluoro-sodic-pedrizite from Tastyg has the following crystal-chemical formula and unit-cell...
Image
Radial aggregates of ferro-pedrizite in albite–quartz matrix. (online version in colour)
Published: 01 June 2015
Fig. 1. Radial aggregates of ferro-pedrizite in albite–quartz matrix. (online version in colour)
Image
The crystal structure of ferro-pedrizite: projection onto (001). (online version in colour)
Published: 01 June 2015
Fig. 5. The crystal structure of ferro-pedrizite: projection onto (001). (online version in colour)
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Mössbauer spectrum of ferro-pedrizite obtained at room temperature (circles). Four doublets and their superposition are shown with curves.
Published: 01 June 2015
Fig. 3. Mössbauer spectrum of ferro-pedrizite obtained at room temperature (circles). Four doublets and their superposition are shown with curves.
Image
An amphibole composition space based on generalized tschermakite, edenite and glaucophane substitution vectors. (a) The planes edenite–richterite–pedrizite–glaucophane and tremolite–richterite–edenite are limits of amphibole composition. The planes tremolite–edenite–Al-Mg-sadanagaite–tschermakite, winchite–richterite–Mg-taramite–Al–barroisite and glaucophane–eckermannite–nyböite mark the calcic, sodic-calcic and sodic amphibole groups. The glaucophane–pedrizite–Al-Mg-sadanagaite–tschermakite is not a fixed limit of amphibole composition space; for example, the presence of R4+ cations at M(2) would permit values along the tschermakite vector that extend beyond this plane. (b) The dark gray planes show constant Si content and the lighter gray planes show constant CR2+ and CR3+ in this amphibole composition space.
Published: 01 October 2007
Figure 1. An amphibole composition space based on generalized tschermakite , edenite and glaucophane substitution vectors . ( a ) The planes edenite–richterite–pedrizite–glaucophane and tremolite–richterite–edenite are limits of amphibole composition. The planes tremolite–edenite–Al-Mg
Image
Optical absorption spectra of ferro-pedrizite, obtained with the polarization E ∥ c (a) and E ⊥ c (b). (online version in colour)
Published: 01 June 2015
Fig. 4. Optical absorption spectra of ferro-pedrizite, obtained with the polarization E ∥ c (a) and E ⊥ c (b). (online version in colour)
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Powder infrared absorption spectrum of ferro-pedrizite: (a) general view; (b) close-up in the region of O–H stretching vibrations.
Published: 01 June 2015
Fig. 2. Powder infrared absorption spectrum of ferro-pedrizite: (a) general view; (b) close-up in the region of O–H stretching vibrations.
Image
Variation in Li content as a function of F content in Kajlidongri amphiboles (black circles) and fluoro-sodic-pedrizite (white circle); the straight line denotes the leastsquares fit to the data.
Published: 01 April 2008
F ig . 9. Variation in Li content as a function of F content in Kajlidongri amphiboles (black circles) and fluoro-sodic-pedrizite (white circle); the straight line denotes the leastsquares fit to the data.
Image
The relationship between the strip of M(1–3) octahedra (populated by C cations) and the double-chain of T(1–2) tetrahedra (populated by T cations) in ferro-pedrizite. (online version in colour)
Published: 01 June 2015
Fig. 6. The relationship between the strip of M (1–3) octahedra (populated by C cations) and the double-chain of T (1–2) tetrahedra (populated by T cations) in ferro-pedrizite. (online version in colour)
Journal Article
Published: 01 June 2009
Mineralogical Magazine (2009) 73 (3): 487–494.
...{document} Al 2 Li) T Si 8 O 22 W F 2 , is related to the theoretical end-member `sodic-pedrizite', A Na B Li 2 C (Mg 2 Al 2 Li) T Si 8 O 22 W (OH) 2 , by the substitutions C Fe 2+ → C Mg and W F → W (OH). * E-mail: [email protected] 7 7 2009 14 5 2009 © The Mineralogical...
Journal Article
Published: 01 October 2004
Mineralogical Magazine (2004) 68 (5): 825–830.
..., which cannot be fitted into the four major amphibole groups. New root-names such as sodic-pedrizite in the Mg-Fe-Mn-Li group and obertiite and dellaventuraite in the sodic group along with two new prefixes, parvo and magno have also been added. As result it has become necessary to modify the AMPH-IMA97...
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Journal Article
Published: 01 March 2003
European Journal of Mineralogy (2003) 15 (2): 309–319.
...: leakeite, kornite, whittakerite and pedrizite) have more than half-occupied A-group sites. Seven new amphibole end-members containing lithium have been discovered in epysienites (dequartzified and albitised granites) from the Pedriza Massif (Central Spain), where lithium incorporation and partitioning...
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Journal Article
Published: 01 July 2002
American Mineralogist (2002) 87 (7): 976–982.
...). It contains the maximum amount of Li that can be incorporated in the amphibole structure. The name was approved by the IMA-CNMMN together with restriction of the use of the prefix sodic in the pedrizite series to compositions with B Na > 0.5 apfu; its use for compositions with Na tot > 0.5 apfu has been...
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Journal Article
Published: 01 March 2000
American Mineralogist (2000) 85 (3-4): 578–585.
...} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(^{A}(Na_{0.70}K_{0.03})^{B}(Li_{1.34}Na_{0.58}Ca_{0.08})\ (Mg_{1.75}Fe_{1.65}^{3+}Li_{0.88}Fe_{0.32}^{2+}A1_{0.21}Ti_{0.11}Mn_{0.07}^{2+}Zn_{0.01})Si_{8.00}O_{22}(OH_{1.35}F_{0.65})\) \end{document} . Structure refinement of one crystal of pedrizite...
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Journal Article
Published: 01 October 2007
Reviews in Mineralogy and Geochemistry (2007) 67 (1): 55–88.
... Li in the magnesium-iron-manganese-lithium group. Lithium is an alkali metal, is formally monovalent, and shows complete solid-solution with Na at the M (4) site in monoclinic amphiboles, e.g., leakeite–pedrizite: Na Na 2 (Fe 3+ 2 Mg 2 Li) Si 8 O 22 (OH) 2 – Na Li 2 (Fe 3+ 2 Mg 2 Li) Si 8...
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Journal Article
Published: 01 December 2003
The Canadian Mineralogist (2003) 41 (6): 1345–1354.
..., namely ferri-clinoferroholmquistite (IMA–CNMMN 2001–066) and sodic-ferri-ferro-pedrizite (IMA–CNMMN 2001–068). Many changes were done in the nomenclature of the Li-rich amphiboles in an attempt to rationalize the various problems that arose as a result of the latest findings. Therefore, we provide...
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Journal Article
Published: 01 February 2006
The Canadian Mineralogist (2006) 44 (1): 1–21.
...-chemical or chemical reason for including Li in the magnesium–iron–manganese – lithium group. Lithium is an alkali metal, is formally monovalent, and shows complete solid-solution with Na at the M (4) site in monoclinic amphiboles ( e.g. , leakeite–pedrizite: Na Na 2 [Fe 3+ 2 Mg 2 Li] Si 8 O 22...
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Journal Article
Published: 01 July 2016
American Mineralogist (2016) 101 (7): 1709–1716.
..., 79, 1073–1087. This New Mineral Names has entries for 18 new minerals, including aradite, chlorkyuygenite, chubarovite, cryobostryxite, ferriakasakaite-(La), ferriandrosite-(La), ferro-pedrizite, flamite, flinteite, fluorchegemite, fluorkyuygenite, fluormayenite, fluor-tsilaisite, gatedalite...
Journal Article
Published: 01 May 2004
American Mineralogist (2004) 89 (5-6): 883–887.
...}\ (LiFe^{2+}_{2}Fe^{3+}Al)\ Si_{8}\ O_{22}\ (OH)_{2}.\] \end{document} The prefix sodic is derived from the IMA97 rules for the use of prefixes in which sodic applies in Group 1 only, and then only to samples with total Na > 0.50 apfu. Those with total Na ≤ 0.50 apfu are pedrizite unless K...
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